"The deposits described are steeply dipping tabular masses of disseminated chromite in a serpentinite, with or without associated blocks and sack-form bodies of massive chromite. . . . The manner of occurrence indicates the chromite was carried in as solid masses and crystals during emplacement of the ultramafic host rock. Late movements resulted in shearing and fracturing of ore bodies and country rock; serpentinization accompanied or followed the shearing.

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